


pt hai rot der ects es mea leks Singacllnd hk eertriae ator esd 
ae ee 


MMO} i Be cs 


L. j 
eres Sas eae ere 5 ave aa oe ewae * 


NORTH ub mR CAN. CORDILLE a ae 





ie Yr h uN T H PAR ‘A LBL. 
REGINALD Al DWORTH. i. DA aL o a 


0 kUmeuA cere REE ; a3 EF 


“GE 01 Rolerey ve SURVEY 
DEPARTMENT OF MINES: 
: OTTAWA. 


L012: 


THE UNIVERSITY 
OF ILLINOIS 
LIBRARY 















esette 












an ‘\ 
N¥> \, 

ors Ss vod; 

‘M) 





L y é 
& py f 
eee Iv, fin 





on 





COLUMBIA 


per Pat ie . 


LAVA PLAIN cy 


Sy 








Kry SuHowing PostrioN oF SHEETS. 


OZ ‘UOJ JO SOM SOJIW pG'O SI GL JUOWNUO|Y AJepunog 


WNLVdes 


AXAV1 SVWNS ‘Zt LAAHS 











20’ 
































LEGEND 

























o5 





PLEISTO 
AND RE 


yy 


YY, 
if 

Yh) 
i; 


f 
ip 


YY 


Y 





g 
EOCENE 
Fr ie ee 








—_—_—_—_———_ 





RBONIFEROUS Triassic 












































































Ke 
AS 7 4 
* SY r 
AY ea] 
Svonas diorite - 4 
TAT } 
Sz TUL , a 
a : 
= — 
3 
gical b | Z 2 ees 2 7 “h as: 
ks TERNATIONAL fi BOUNDARY 





Ws etrsessrecetceneny | 
it 








) é —— —————— 
a | { . at ee = ; 
/ ert ( bE a 



























































a | | + _) an \ 
I a “aa Sens fh = Poe A | 
| A f—+——_—_ — im 
ies [ | oa ] = 
} lee / 
Note. Localities of chemically analyzed y i= ay, 
rocks, shown thus, +201 ‘. | — | iS 
H 4 
VA ae re |e. | 
No RTHWoop — Vas eG. EAREROOK | 
i | 
{ 






















































































lopography from surveys made by 
the Boundary MIMALSSion. 


Lake 


















reich sae! Section along Ine AB 


GEOLOGY OF THE EORTY-NINTH PARALEE ie By R.A.Daly. 
Scale : 62500 — 0.9864 Statute Miles to lInch 








Miles 
MAP 90A 
Contour interval, 100 feet Reprinted. by permission of Chie? Astronomer, 


to accompany Geological Survey Memow N?°38 


‘ae c | + 
ey PR ey MOG eR yt 
RE Raa, hk RR Bnet ey 

=i 7 ae he a . 


Te 


ee 





(0) 


TRIASSIC CRETACEOUS 


BONIFE! 
ee ECARBONIEEROUS TRIASSIC 


@) 
MIOCENE 


a 


(?) 
CARBONIFEROUS 

















: Z Sheet N° I6. 
12200’ ee. 


La 4 , Vs 
65 60 45 40° 35° 
































Alluvium 


LEGEND 











bit 
a 
© 





IY 
a 
yy) 


yp 





} J 


dark eas ae 5 ; D beds of grit 
7 Inter: , 
TM ES conglomerate Ae 


zy Vga 


il 


=) 





i ac formation ; i / / = \ \\ NS B —\/ WY MVA 
chiefly flows Bi hee and hornblende 300 = Sx 
andesites, ash-beds ih So Z 
























: hilliwack Series “ee 
Liite , quotzitic sandstone, and estore, 
SLE cer Deda tof grit! conigLorwercto 
Intrusive 
| 
| 
| 
Chilliwack b: Hith | 
granodiorite , with gredtic phases | 








Slesse stock 
Monit 


, 
yy 


ih | (iif , " = wee G 
tn a Li ta yale 
Vedder greenstone S Ny / Mi ) Ms Z Deas aC a 


a ae 


Symbols > 
4 Y; f ww 
4 AS 








ae 7| all EM (san: ~ ‘ \ KEG Lh A HIU| aN : 4 N SK A Ly aS NS s ce IL NA o 
Geological boundary } aa SS Z} Ws ys - fas A ‘ SS SSS : .3 + 49 
gi = { SY y (AS }, ? e LL a ZV ING 5K } (zi = ==e DAR - : K 1 \ 00’ 

















Fanlt 





Note; Structure of Gitus formation, 
Ss 7 on section,merely diagram- 





Localities of chemically analyzed 
rocks, shown thas, + 54 























| | | | | | | 
| Mie N | | | 











12200’ 55 50! = , 


















































lopographs from surs evs made hy 
th oundary Commission 


Probable fart 














ff it 


Section along ine ABC 
GE@GEOGAZORSTHEeFOR LYSNINTH PARALLEL, By R.A. Daly. 


Scale: ezt00— 0.9864 Statute Miles tollnch 
Miles a 


1 % oO 1 3 Ai MAP 89A 
= SS —_ 


———————— EE 











Repriuted. by pernusston of Chief Astronomer, 
; to accompany Geological Survey Memow N° 38 
Contour interval, 100 feet a I : 


aT SPDT ETON POT 


iih 









ae eatiae Ah ohep wrt ‘si 
1s ageborcta >: 
ae 


MELD 


al 







PPOMAey 
ona | 








: 
i 
} 
Ye 
} 
ye ‘3 
My gah ig + 
' as of 
: .] 
4 
: RS 
= hy 
i , u Les 
\ ae 5 
j ‘v4 es a4 
‘ ayts H Pa) 
‘ Deo f 
'y 
a. 
; as an 
a) ¥ 
>? V4 i a A f 
§ J j Py 
| is ‘ P y ; x 
epee Ra eRe, , a ; * a 
. in lie lw 4 ¢ 
’ 7) OY to. | 1 ef}. 
: Nae PAYS Patt; 
Reeth ea cae } : ae 
baa bine cu 7 | 
Ly } Th baTh ‘ i 4 ‘ 
WAR is Jaa . : 7 
ve * ek ae ; z 
P + 
AD + aa P| tn linn ape lane nthe kee bay Uy at eae 
y 7 > A ‘ . ‘ yma mma rt eeday tm 9 = even 
i Iskzo, 
4 P * Rrcnarsomie een eae me Ftc ey 
ae 
5 
} 
‘ 
' , 





PLEISTOCENE 
& RECENT 


OLIGOCENE() 


CARBONIFEROUS 
YF 


( 
CARBONIFEROUS 


MIOCENE () 
$F 


0) 


JURASSIC(*) 
—_, 


LEGEND 











eee 
oe - 
Glacial striae 


Note. Structure of Hozomeen series, shown 
o 


n section, merely diagrammatic 








| ‘Ny if | : DS J > K > >») Sy EN 
F S \ Na) 
IGEN \ | 














Sheet NY 15 








10’ ae 12100" 








L130’ 25/ 20' 














f | | Tl 








49° 
On 















JAY 
Tee SSN 


ay 
ave 











aif 05 


HOZOMEEN RANGE | 











? 

















r 2 ti 
J Ly i S. & : 
Zam 





a 


(ZAC 
Tie NS 
a 
; \e 


Nt 
Ny \\ 


y} 
y 






































Le —— SS t = 
I2130 ra 20° 15’ 5! —— 
—_EEE SSS 2 = ee ee — — a = 
Topography fram SUTVEVS made by 1274 
th Boundary Commission. 
v TI. ; 
A 3) — tft} “ae 
Rs 8 7 ot aca ] tty 
= Sas oS ti Vt — 
by pS) ge Lf} Se 
i i ST = 
oi By = SEK K KKK KI fo 
Sy RX XOX KT 
ees ‘KX KX KK KK 
DX KR XX KKK x 
KKK KX XK & Xx 
KX KKK WK KOK 
CXXXXXKKK NYS a. ee 





















Section along line A B 
GEOLOGY OF THE FORTY-NINTH PARALLEL, ByR.A.Daly. 


Scale: 62500— 0.9864 Statute Miles tol Inch 
Miles 


L % Oo 1 
SSS ——— 

















Contour interval, 100 feet 














MAP 88A 


Reprinted. by permisston of Chief Astronomer: 
to accompany Geological Survey Memoir N°38 
s « 


: Le 
1 

i: oF 
i 
aa} 
3 
ii 
Di 
if 
i 

| 








& 1 é 








= 


Jer ai ranoN ia 


tenth 
AW SSe iC Nue RT, BME “ti : 







i 





We ate 


“Le didium 


sete 
i i sit 


Aen abe 4 


rik Sint ce 
ne i, Shjtelia Sajna 


i ai 


% 


i 





Pint Vay eet iting: 
a 


a ' Ey | 4 
tasks roe? 


Ameer ae 


air, lo js bite 4 


) abbrose sartetvassoneyd Oh OAS tM Neda tes sy mstre. eee x) 


: Ni 


a eens h A en pcan age? 


MS RS 


¥ 
<= 


SU ACEH 
iB 


2 Y88e-CHICO) 
CHE LYCEONe 





s 
ae 
SN 


of 





{ 
he 
»  hlad 
> 
oi 
i © 
wo 
veel 
a 
. 
| me 
ig 
E Oe 
e- 
at ss 





semes 


(SHASTA-CHICO) 
A 


CRETACEOUS 
Pasayten 


—~ 


LO! 


WER 
TACEOUS 


af 





(a) 
CARBONIFEROUS CRE 


ee 


MIOCENE (?) 


co c 


Es 


JURASSIC() 


LEGEND 


Member L 
bi tk argi 


Member K , 
and sandstone with 
mete eda ofateata and conglomerate. 





Members Btol 
arkose and sandstone chiefly, witht 
conglomerate and shale 
ae 


Pasayten volcanic formation, 
andesitic breccia 


zomeen series 
greenstone cherty quartzite & limestone pods 


Intrusive 





Syenite porphyry 
chonolith 


ZZ... 


Castle Mi 
graw 
Lighummg Creek stocks 
diorite 


Remmel batholith 
western phase; sheared yranodiorite 


Symbols 
: 


i | 


Geological boundary 


aR Bee 
Fault 
Pes 
Glacial striae 


Note. Structure of Horomeen series, shown 
i section,merely diagranunatic. 
Localities of seater analyzed 
rocks, shown thas, + \F4l 






































es 
e 
SOQ 
\ \ 
Wks 
NX. 


SER 
Sc 
SA AQn 

. 


a \ \ 
Ne 
O 





SS 
AI 


fp 











SS 
N 
7 . 
4, 





f 


6 
WANS ie 
\ 





— 
2 















‘ \\\ \ 
\ 


\ AS 
RN 


AY 
- SSP SPAT [SN S 
Y { (HT | ~ 
NWRPANN ! 


































SIX 
o LQOO73dy 
SSS NSS S 
2 OF — SS ) 
~~ LAA 
HY, y 


as a 











WS \\ 

SINS NY . SS 
Ss Wh S 
—“—S 5s 


ip (( f 
iq ( 
sae 


78 



















































































is 
LLL IP EE Le 











Contour interval, 100 feet 














22d, OS BSI 
oo 9 on y LSE ID SLO DEA 


| Section along line AB 
GEOLOGY OF THE FORTY-NINTH PARALLEL, 


Scale:62500 — 09864 Statute Miles toll 
Miles 


Reprinted by permission of Chief Astronomer, 
to accompany Geological Survey Memow N° 36 








- 
y ‘ iy i? ' ‘ 7 
pee : at ; 1 , i 
fi ‘ ; f 
‘, ‘ i ; 
1 > » 
i ’ 
, 
‘ Fi » 
{ f 
i ; 
° ve 
} l 
} 
iL 
Hewwe we awl A. eben A tals MR OAD AO ELE AA RA PERE PE RRAD Ea Mig Rler 0 vist th raewrntiwy 14 eee ne ame mete poarlrepbingnantier tore, ohne He 
i wes sty rat ‘ hate eA % , (a ye a Be a 
i eR rte late ete ee OaE Dp Ni MP, fer Pact A i eS Mh mys ethno ' 





sty 
% 


wi scrtmiaaarlesiigahe i C - eat NAN Me se hae FH tony A my ee el NY et po 
re rrpmwt cand tates or creases aioe a rasa Be ero ere ve ere tnt gh ates ng ie ial ol ber Lidkainn Likeein Late een eee hee belt 
t i ‘ , i 


4 5 t mt ‘ 


hae 
iioapaeal 


Dera a 
sek: Bite 










ls "y 
Aen ye 1M ahea 


ai 


ase 


be 
7E 


es 
—<— 


MSIF od 2 


e 


f 


a be eiales heh ooh Spe fn aie ama wae) 





rcetbnrtarmenty rt i ae 


LEGEND 











& 

Fe 

oS 

e 

3 | Vesicular dikes of basalt (BauermunRidge) 
a | and andesite (cutting Basic Complex) 
> Park granite stocks 

s 

Fr 

a 

wW 

= 





Nf, 2 oe. 
Si 
sh ees 


Agglomerate 


LOWER 
CRETACEOUS 
a 


Remmel batholith ; 
zeae pee highly salic derivative 
sheared granodisrite 


oy Ee 


Remmel batholith 
Western phase; sheared granodiorite 


Ashnola gabbro 


—— 





Basic complex 


LATE PALAEOZQIC@) JURASSIC (?) 


Symbols 


Geological boundary 


ae 
Glacial striae 


Localities of chemically analyzed 
NE ee Sse OO 























y) S , 


fe (S y) 2 AMY " ne ‘ 
ae Ml ( Bo ge 
AL (( (G = NS sa =e ZZ 
Cer ase 


ees 


A = . q 
7 —~ 





















































W A S H ( ue O N 
— — = = = = = = — = ————— << =f —= ———————[—————_ = = — = ——— & I = _| 
25’ 20’ 1 10 ~ 6 12000 


120 30’ 








a“ 








Lopography fr surveys made by 
Be Saris + Comodo. 








Section along line AB 








MAP 864A 
GEOLOGY OF THE FORTY-NINTH PARALLEL, By R.A.Daly. T= 
Reprinted by permission of Chief Astronomer; 
Scale; aztoo = 09864 Statute Miles to 1] Inch to accompany Geological Survey Memoir N° 38 
Miles 




















Contour tnrterval, 100 feet 














waa! 
te Un Ba 


Sp ait nha de 


Sikemadcsihidedioteioteee seated 


bb Aere-iirsiesibiy hess tans nellionseglens clon 





ar A 
i el 4 
4 4 pido / 
Wiey t Pith 
* yy s 
t 
? 
¥, 
; om, 
7 
¥ ats 


; dairy % “ 5 a xd 
on 


oa Sa 


‘ 
Ph. 







st) APachan teeta 


el hal ee ee 










* ” + ao 4 hee fine 


ei ciends, Oe Ay. Fate hg ete. 











35° 


40' 








INTERIOR PLATEAUS 


BELT OF 








45’ 


50° 


6b’ 





OSOYOOS 


\) 
W\\\\\ 


NY 


\\ 
\\\ 


\\ 

NARA 
\\\\) 

\\ AY \\\ 








Says. aE M ) 








(c ARSC Ay DLE 


RANGE 








12000’ 





O K AN AG AN 


4 
\\ 
4 
EX\| 


YY / Ae 


CELL 
 Caeioyaoe, 











a 


| 
if 


\ | 
\ \eN) 
WV 





4 


<] 


Y 


Wy 


<= 


4-700 








LEGEND 


— es 


y) 


Intrustve 


4 
B= 
i 
i. 
7. 
E 


matignite and eleolite Syertite 





4N399Y % (JOIOZOAVIV 


INIIOLSIFTd 


Yaddn 


AYVWILY AL 


—} 


— 


Osoyoos 


gneissic batholith 








Peridoute 





(orssvunr (Jo1oz0avIVE 


aLvi 


yinbols 


“ 


8 


J 


Geological boundary 


aS 


Glacial striae 





CHOPAKA Mt 









































is 
Nu 
a 
g 
of 
5 
| 
| 
| 
| 
| 
| 
Wr 
iit ive) 
| 
| 
| 
| 
eee 
So |i 
oe | 
1} -H 
| | 
| 
| 
| | 
| i 
i} 
| 
}] a! 
| | 
| 
| 
| 
| 
a 
ive} 
H 
| 
| 
| 
4 
| 
| 
Tl 
| 
| 
| 
\| 
\| 
i 
i 
Ss 
Ne 
i} 
| 
| 
| | 
| | 
| | 
| 
| 
| 
|| 
| 
| 
| 
| | 
| 
A 
| io 
a Te) 
it B | 
| | 
| | 
| | 
| 
| 
| 
| 
(YT 
try P16 
> 
Ry) 
aC 
s : 
NaS 
aS) 
a) 
% 
AH 
2.4 
| a 
33 
aE 
-8 
a 
§ 
BS re 
SS 3 
s ages 
S iss 
°' y 
AS 
S 38 
38 
N 
y 
scone | SPS 


D1 section, merely Hagraranatic, 


Locahities of chemicall 


Note. Structure of Anarchist series, shown 


anal yzed 


shown thics, +\|00 


Ly 


rocks, 














QW 


MIAN UBIULIY TUNG 


| 
| 
| 


AB 


GEOLOGY OF THE FORTY-NINTH PARALLEL, 


Sea rae, 











Section along lne 
© 


By R.A.Daly. 


= 09864 Statute Miles to | Inch 


= 
62500 


Seale: 


Miles 





MAP 85A 


Repruuted by permission of Chief Astronomer, 
to accompany Geological Survey Memoir N?°38 


Contour trterval, 100 feet 


BY v 
we : s 
avin. Lannie eat" 

ao - 


YaRAQwudses 
4k ¥) 
Sees Sot cnrereeee eee OS ren 


- 


ALeG' Vv 'M 


—<tl 7 Wr sat Re 





\ f al * 
Mea 4 Sei a” 


(?) 


P, ReOzOIC 


(7) 
CARBON- 


PALAEOQZOIC IFEROUS OLIGOCENE 


U PPER 


ME RECENT 
BRE 


(?) 
MIOCENE 





(?) 
JURASSIC 


a 





Note: Structumes of Anarchist series, shown or 


(?) 
MIOCENE 
Rely ee 


— 


LEGEND 






Shackanite 


flows (part of Midway voleanic group) 


Exrrusive rhomb-+ 


flows (part of Midway volcanic group) 


= 4 SS 
Kettle river formation. 
sandstone, conglomerate, shale,arkose 






Limestone of Anarchist series 
white to bhdsh-grey,crystaline 


An 


Intrusive 


Intrusive rbomb-porphy 
chonelitiis und dikes 


Oscyoos batholith 
gneissic derivative of granodiorite 


Diorite and gabbro 


Dunite 
Symbols 


Geolo gical boundary 
a 
Glacial striae 


the section , merely Hagravonatic 


Localities of chemically analyred 
255 


rocks, shown this, + 








10" Pe es Ss MIDWAY MOUNTAINS 




















N 

[> 
we 

(080 


a 
f 


a 


008 
jl 
LY, 








11930’ 






























































Topography from surveys made by 


the Boundary 





Commis ston. 


2 
49° 
00 
20° 15 10 5 T1900 
>>. ae B ee _ 


LORS 











Section along Ime ABC 
GEOLOGY OF THE FORTY-NINTH PARALLEL, By R.A.Daly. 
Scale: 6z500— 09864 Statute Miles tolnch 











Miles 
1 % ° 1 2 3 4 
SSS SS SSS =e rs 
Contour tnterval, LOO feet 
yniti erve MAP 84A 


Repruvted by permission of Chae’ Astronomer, 
to accompany Geological Survey Memow N?36 











bene 


Téye Al 


7 . 





f AY, 


mh She f ARS 

Sa! —— 
YAAaKHY Ge 
ON a . ae te! o.) RS ag 
PS Rep Soe 8 Sn An Shs SANTI 2A LS a a en eee tee ee 


‘— 


SAG ONE wAregy usd (131) 








PLEISTOCENE 


OLIGOCENE MIOCENE & RECENT 


(?) 


“ 


(?) 


CARBONIFEROUS 


(?) 


?) 


A 


() 


CARBONIFEROUS JUR, 


RBONIFEROUS 
0 TRIASSIC 


SSIC OLIGOCENE MI 


ey ee 


aon anata 


aE! 


Q 


(a) 





OCENE 
Pen 


iene 


= 


flows and pyroclastic deposits 


LEGEND 


| cee aie | 


Alloviuin and glacial daift 
f ae 
Midway volcanic Same 


tnachyte Sats ote ptr rhomb-porphyry ; 


flows and pyroclastic deposits 
Me | 


Midway volcanic group 


andesites and basalt;flows end pyroclastic 


abs 
Kettle river formation. 
sandstone, congluinerate,shale,arkose 





S Px zs 


Phoenixvole formation 





LZ 
Attwood series 
argiltite , quartrite , limestone 
An | 
prone series 
quartzite, phyliitic shales, greemstones with 
‘ers Pireston eoodes 





i 
ovystalline ,bliiish-grey to white 
Chlorite and hornblende schist 


Grand Forks schist 
anphibotite, hornblende schists,ete 
Intrusive 
Pulaskite nyrry 
kiana gilts 
RKhomb — porphyry 
rite 
chonoliths, aye and sills 


Granodiorite 
stocks , dikes,etc 


of augite andesite ete 





Sheet N10 

















_ (COLUMBIA. 



































ER NAOT Ie NN 





118307 
























































Lopography from surveys made by 


















the Boundary Commission 
Serpentine 
ihes,ete By 
Symbols od 
| ane! z £- aa = 
Geological boundary ——_ ke Pals 
—— SO ee as 
See ore ris 
Sea Leve/ : SE [EX ee 





Glacial striae 





Section re line A B C f 
mee sce, hem nn rns rl GEOLOGY OF THE FORTY-NINTH PARALLEL, 


Gagrarmatic. On account of the small scale, 


modiorite apophyses are se 
Scale: aztoo — 09864 Statute Miles tol Inch 





porphyries, as well as 


not plotted. Simalarly many dikes which aresyngenelic 
with. the volcanics are not shown : 
Locahities of chemically analyzed 1 % 6 : Miles Z : ‘ 
[as —— a —— se —— os 1 = —— Scant = = ————oe x SS — ———— — 
MAP 83A 

















rocks, shown thas, +\0\0 
Reprinted. by permission of Chief Astronomers, 


Contour tnterval, 100 feet 
to accompany Geological Survey Memotr N?°38 


ViATMUOM* anAse 





TERTIARY 


CARBONIFEROUS 
TO CRETACEOUS(’) 





PALAEOZOIC() 


(°) 
CARBONIFEROUS 
“~__—_, 


(?) 


MIOCENE(?) 


EOCENE?) 


a 





CRE TACEOUS®) 





JURASSIC(’) 


LEGEND 


Conglomerate 






Phoenix volcanic formation. 
flows and pyroclastic deposits 
of augite andesites, ctr. 


Rossland volcanic formation. 
flows and pyroclastic deposits of latites, 
andesites and basalt. 


Par | 
jeu 


Sutherland schists 
phyllite, garnetiterous, pidotic and 
achnolitic schists, etc 














Liamestone 
white to bhash marble 


Grand Forks schists 
amphibotite, hornblende schists etc 


Intrusive 


Coryell batholith 


hornblende-biotite syerite (pudaskite ) 


Syemite porphyry 


peripheral/younger) phase of Corvell batholith 


Olivine syenite 


ee 





Smelter stock 
aplitic grarite 


[ } 
| 
Cascade batholith 


gneissic biotite qrumiute : satellitic” 
stock south of Castle mountam 


Symbols 
bers 
( seological boundary 
—-> 


Glacial striae 


Folded structure of Sutherland. and. Grand Forks 
schists, in sectio: < pee ee 


Many apophysal dikes from 


large intusive masses 
not shown : 


Localities of chemically analyzed 
rocks, shown thacs, + 5\7 : 






































































































| 
Jao la 
ah 

| 

L 





a — = - = = ————— == 


11830° 25° 





r 
| 





Topography from surveys made by 
Commisston 


the Boundary 


 \Gramnby Smelter 























piney 











een i ooh) 
Gre AiO 
sas anton fo 358< a} 
7 





<1 


PSE RON As alnOunc-s 1 








GEOLOGY }OF 


1 


SE 


#3} . ( pets: 
es) (] be \\ \(\ i | : eee, ——S : TR 
LU UU peal 


20 ei 
15 10’ 
y » 
oOo Ba eee ese eee ee 2 s fs 
Feces \ 5 a 8 
\ fhe pve aa TT, ES & & 
oo ae 
byy ae fet } } aS } ] fi] S ) ee a /\\ 1, / be, 
coe eeee 8 : KOA Rv 


> 3 








11830’ ‘ 
25 20' ‘ 
eee | i . a ; 1b ROSSLAND 10 MOUNTAINS_ sizJCOLUMBIA 5 SYSTEM) 
| 
| | 
| 
| | 
| 
| 
| 
| 
| 
| | | 
4.9°| | 
Pos’ |i : ~~ ip i - . ae 
| | 
| Ca oR, 1s sat ily, NSA RANGE Ce oven iA Ss¥as: Vice My) 





ROSSLAND 





Section along line AB 
THE FORTY-NINTH PARALLEL, By R.A.Daly. 


Seale: azboo — 09864 Statute Miles to | Inch 
a. = SS = Z heats 








——— 





Contour interval, 500 feet 


49° 






























169 | 


MOU Rak 


















MAP 82A 


Reprinted. by permisstorn of Chief Astronomer, 
to accompany Geological Survey Memoir N° 38 





LEGEND 


Conglomerate 
fossitiferous on Sophie mountain 


Beaver mountain sediments 
grey and brown shales and sandstones 


TERTIARY 


Beaver mountaim volcanics 
we and py z zt c 
ui and basalt 






(?) 
CARBONIFEROUS 


ETACEOUS TO CRETACEOUS 


Sx 
Rossland volcanic formation. 
flows and i its of latites, 
basalt 


Lowen 


Carbonaceous argillite, sandstone,etc. 
fossitiferous 


Pend D'Oreille limestone 
white marble, fossiliferous 


CARBONIFEROUS ¢ p 





(2) 
CARBONIFEROUS 


beperice 
Pend D'Oreille schist 
Carbonaceaus phy ite, with quartcite 


Intrusive 


TO ORDOVICIAN 


Coryell bathoith 
hornblende-biotite syenite (pulaskite) 
with phases of syefite porphyry 


—. =a 






__ TERTIARY 


Sheppard granite 
biotite granite; stocks and dikes 


Shaiiernzone of Tx baibobib 


Trail batholith 


granodiorite 


MESOZOIC 





Rossland monzonite 
sto. 
7 Dunite and Serpentme 
| dikes and chonoliths 
Symbols 


— 


Geological boundary 





Note: Many mincttes and other micalamprophyres cut the 
Pend DOreille schists in the Pend VOreille river gorge, 
as well as the older rocks in the Rossland waning camp. 
Numerous porphyrite dikes syngenetic with the Rossland , 
yoleanics are not shown and apophysal dikes trom 
batholiths and. stocks are tikewise not plotted. 


Locahities of chemically analyzed 
rocks, shown thas, +409 : 


Sheet N? 8. 
1 








ROSSLAN D 55’ 


_ 4 SELKIRK VALLEY £0 


(SELKIRKS)  Il730' 
7 








MOUNTAIN 

















oe) 










































































































































49° |[T_1 , 
os’ 49 
oy 
| 
| 
49° (| 
00 | Le ——— Bt A | 49 
00’ 
ROSSLAND MOUNTAIN'S COLUMBIA SYSTEM} r 
( /W A Ss H I N G T a x ea | | 
Heb ———————— ——— oo ——————————————— = = SS = — ———— — —-—— =i = ——— ae x = aes = al | 
11800 56 50" ry me es a 
5 30 
1L DOGT" oh 2 fro L surveys made by ri ¥ R 7 aioe a a = = — ——— —— ee = 
i aia: sty eee ot ae ‘ $ 5 § 1267 
ar 8 
> $ 
[ ae = oe — 2 ~ g rs 
: 2 Tae : & g 
A _ en nae 2 eS ee a : § : S 
ie —SS——~” me . 2 : 
| 8 ag Rv RR : 3 \ s 7 
| Rv S a= ae SS a aes = Ss 8 —— ———— 
AS Rv 


Sea Leve/ ae *, Aes SE ee 7 sess = seis eS 














Seetion along line AB 


GEOLOGY OF THE FORPY-NINTH PARALLEL, By R.A.Daly. 


Seale: e2500 = 09864 Stanite Miles to IIuch 


1 Ve » 1 Z a + 
aS SSS eee 





Contour tnterval, 500 feet 


MAP 81A 


Repriuted. by permusstorn of Chief Astronomer, 
to accompany C reological Survey Memotr N° 38 





TERTIARY 


~ 





CARBONIFEROUS 
TO 


ROUS 


To 
BRIAN ORDOVICIAN CARBONIFEROUS CRETACEOUS?) 


() 


CARBONIFE 


MIDDLE CAM 


(?) 
chiefl 





& BELTIAN LOWER CAMBRIAN() 


() 
LOWER CAMBRIAN 





BELy! AN 


(Uk 
TERTIARY 








LEGEND 
BONNINGTON 


(SE Lok I RAK ESE 











ieee 

















Bs 
Beaver Mountain sedimenrs 








Beaver Mountain volcanics 





Rv 
Rossland volcanic formation 


flows and pyroclastic deposits of augite 
andesite and basalt 





Pend D’Oreille limestone 


white to bluish massive marbles 





PD 
Pend D'Oreille schist 


carbonaceous phyllite with quartzitic 
and amphibolitic izterc LOLs 


L 
Lone Star formation 

dork grey, carbonaceous phyllite , with 
quart schist aid quartzite 











Beehive formation. 
banded quartzite, with thin interbeds 











of metarguiiite 











Dew formation, 
banded quartzite, with conglomerate interbeds 


WE 
Wolf formation 
massive grey grit_and arkose in very 
thick beds ;* subordinate sandstone 











Mk 
Monk formation 
alternating phyllites and metamorphosed (schistose, 
guile, sordstoives, aril conglpyterates : Grey colons 
Iv 


Irene volcanic formation 
thick flows of pyroxene ardesites, 
with some pyroclastics 


Intrusive 





Granite 
satellitic to Bayorme batholith 











Symbols 











5 he 
Geolo gical boundary 











oe 

























































































Lopography from. SUTVEVS made by 
the Boundary Commission 


Note: Somewhat r20nerous, though narrow dikes of minette, 
cutting the schists im the Pend DoOreille valley, are not shown 


Note. Locahties of chemically analyzed A 
rocks, shown thats, + 666 . 
































Sea level ae ee aed are = eee 





3 Sa 8 
cay ret a a Pa Tm) 
= » ‘ \ pi au: Va 
a 2 y a Yi : fw) ear HN \ 1 
= 2 Pi, H q0)/ PHN \ 
eT “ 3 \ | Yai DUNN \ 4 
fn \JPoy/ ST Py N \ \v| 
ned A wis oh \ 
JIN | ~~) \ 
i sal ON SOSA a Me 0, maa << SS i ( Nina \ 
Seetion along line ABC 
GEOLOGY OF THE FORTY-NINTH PARALLEL, By R.A. Daly. 
Seale: 62500 — 0-:9864 Statute Miles to LInch 
. Miles 
ee ret — > ee =——_ EE ———— = a ——— MAP 804 


500 feet Reprinted. by permission. of Chief Astronomer, 
. " ay" Py ee - 2 * To ¢ 
Contour interval, 3 to accompany Geological Survey Memoir J 098 


- 
hes dali 


sal a 
Prince rely 


X 


res 7 - p ar pends 
Fawn tae gine ere v 
lentes > : re ae 








ae eee 
se 





ef 
=) 
ra 
alt 
z 
= 
2s | 
siz 
z=: 
S 
| 
2354 
ao 
Ea | 
= 
vA 
< 
F 
Ww 
oO 





—- 


PRE-ge, TIAN PRIEST RIVER TERRANE 


(”) 
© TERTIARY 


( 
JURASSIC. 


(?) 
CAMBRIAN 


(?) 








Sheet N? 6. . 








LEGEND l7d0’ ' if 











T1630 





























Albovium 





Kitchener formation 


greerish-grey quartzite 
wf 
Wolf formation 


massive grey grit and arkose invery 
thick beds; subordinate sandstone 





Mk St Mk 


Monk formation 
altanating phyllites ad metamorphosed (schistose) | 
gris, sandstones and conglomerates; grey colours. | 





f Irene voleanic formation 
trick flows of pyrocene andesites, with some pyroclastics 
and a massive witerbed of magnesian limestone 


Ic 








Irene conglomerate 
massive, greatly sheared; thin sandstone lenses 


























wica schists, guartzites and dolomites 


dolomites, quartzite and. phyllite 


rs 


Phylbtes and sericite-quartz schist 


sheared, massive quartzite, with secricite 


and chloritic schist 

















= 
sericite schist, spangled with large biotite a-ystals 


schistose quartzite and mica schist 


e | | 


glittering mica schists and sheared quartzite 


Intrusive 








& | 
Bayoune batholth | 


Basic granodiorite 


ery 


et 
tykert batholith | 


sheared,porphyritic biotite (raiscovite)grarate 





Abnormal hornblende granite 
probably a sill 

















Abnormal once abbro 


sills in Kitchener formation 

aes ae) | 
| —— | 

[ae eee Al) | 


Greenstone | 
dikes and sheets tn the Priest River terrane 
































: ; i ae, FLPE, LS Pe Fe 
S bols Lopography from surveys made b 
ee the Boundary Commission. 


| | 
| | 






| Uncontornrity 
South Fork of 
Summit Creek 

















8 <x 
pases > = 
Geological boundary 3 = a A 
8 38 ae | gi . 
mee A = \ Pen ER ane ee aie S 
E SOO PTT NN | ae 
Se => \ \ ) | aay tee 
Fault Vie e | : e J j rt ‘ 
: A E \ 
= | Elz 0, 26 : E 
Glacial striae os } a a Be) 
a= 7) eg eile ee o- 2 os = = = ——s = = = —_ and = be = 























Note. Structure of Pre-Beltian series, shown 
on section, merely diagrammatic. 
Localities of chemically analyzed 
rocks, shown this, +9 


L V2 oO it 











Contour interval 


Section a long line 


GEOLOGY OFSTHeEeEORLYONINTH PARALLEL, By R.A. Daly. 


Seale: 62500 — 0:9864 Statute Miles to LInch 
Miles 


SSS = = = $1 


AB 


500 feet 


























iN eS . 
‘ WAL Ss % \ 
Pray Lay * 


walt 4 


wu u “Si 4 
: wilt r 








Port Hi 
TRENCH | 








1265 

Ny 

5 

< 

— > 
> 

& 

8 

$ 
_ ae SB 


MAP 794A 


Reprinted. by permission of Chief Astronomer, 
to accompany Geological Survey Memow N° 38 





ony hip cen erence 0 tet TN a IE LRP ASAI AEST ~ ” 
- - . eerielipn atin tat fill ar oan Lt GE OE ECT A | 


“ 





Sear 


ET Sete + 
ee 
jeans ee cae * 





oe he | @eqyu‘e “131 


{ 



















inp Me 
: . “ C Px ; Sas sak incense te lated ee iy oh fr NO IS 
° : nt ent lh ae a tae le aml Ah 

; 7 te : = a . i Uy ‘ = 7 7 

*. . fn . ud ¢ . “ae 
rae all Le eae ae ee we is Qe i a hee 
SMT Wel Pk ik RR Menke Tht yh , 
fue eeat 3 ; ae as 
hy ina roe 
prrerpetse ita stemnnya liom ay ig (a one in 



















































: “25 15 10’ 11600’ 
LEGEND | cz - coe a : & | age is = | 
PURC | | | 
| = i i mR EN) CoH : rn M 0 7 E . nm Ss 4 E Y iS K | R A N G E 
aI | | 
Cp (d) | { fa 
= | | Wit x 
) We 77S Si er 
s x oan \ MN; YO KK ay ‘ iS 
thia-t . 5 } s R x fo Zz “& ¥ ne ANY, Y AN ( os mp 
V3) S SS) S/N ! GSS ie ; eum 
Ke Yb 27 S My Z\\ NOMI, Al NE L\( A \- Mi 
C0 end trtatetantmetegiea a. Wie f Pal Gea AWS \ is We 
: Wy) . | IS 9 S NS NS 
ston formation 7 Yr. tL | SS ‘ : 
“pay ane mem oe as 49 NU \ 
Intrusive ~ > ai ah 
eS 5 


| | 


| 














g 
3), 
| 
| 
1] 
| 
| 





























iii ‘S SQ 2 WK \ - 
e i & \ \ : | BN . = . . aS) S iN %\\\ % CSRS \ a i RT} \ 
\ ay Y \. ae NY \ & )} eS Wes SW \, mG i \ alk \ | | 3 14 Vn \ ; 2 
< WWYQyii Viyep ed), YN ie An i WSs \S a\ PALL WAXr X \ I | | | AN 
¢ \ 3(\ 2 3 ee | | | | IAS 
| | | de 
| 





— = = ———— ———— ———— SS SSS = 
11630 25/ ' , ; 


(| 
———4} 











| : 10 5 600’ 
Topography from surveys made by ae 7 Sap mee ear cee ee a : = = = —— = - Se Seoer see = = SS = — - 
the Boundary Commission. 











ASA 

















Section along ae AB 
GEOLOGY OF THE FORTY-NINTH PARALLEL, By R.A.Daly. 
Seale ezso0 — 0:9864 Statute Miles to 1 Inch 

Miles 


1 Ve o 
Sana = SS es 








= t4 ‘ = 





‘ 


TAA Viushod | 2M 


 S1bP Moe oe eee 









































li6o 40° ‘ 
LE END - Z : ; a — | ii : ee — - ——————————— — — —_—— = a — —_ = = - - oo —— — — i ———— = = —_ = — - — — at 
ee Pe NOT Y A H K Rul A@eIN: <Geae | oo Mico} G Slee ales Re Ae RANGE 
Esai a De ae } % | | 
: | | 
| 











See tee eeace oe eee iterséome dalomite ooh y 
at base (Equivalent pigments oF dots formation) r Y gt: WF Wy / 
WAZ iC WV, 
M GO 
! We a ° 
cy ; ’ 





i 


SS 

VLG 
KA ~S, 
ia 
LZ 


Foe 
pr? 





, 
Gi ya 
ie 
\ 
\ 


renee amin: SAN xe 7 


4 


= 





= 
> 
© 





ys =~ 
= ie | 
(IN 


A 





WY 49° 


eT D 


Sy) re 2 

ee tA NBS 

hy 
oH WN! 

r x { 
H 
oH : : 
lass A 
n 5 
3 ce — 
i : 4 
n SAS/7 
+] 
N 
. 
S 


Ze 


Wir 


HVA 
iS 


> 
SS 


| 








Yahk River ee 


c 
Ss 
<= 
8 
i 


BE) ra 
s 















































Glacial striae 
hittes of chemic. anal, 
Se eras Ete 














Section on hne AB 
GEOLOGY OF THE FORTY-NINTA-PARSLLEEL. By R.A. Daly. 
Scale: 62500 — 0-9864 StatuteMiles to | Inch 


es —— 
















a yi ‘ * 
: . x“ ‘ 
. oe erates setts Se oe en la walvanenienh tea H hethdlcett Aiea.) a dnp ake ip ea «pence shhnadteindamioe tie Hays >. atonrl ta emma har PA rT Laremeas®, (ie PT OT: 
: eh ' ott se ia , 
4 * ; 
‘Oe 
re Sa eta ie i iS etl rena ys hntay EF 9 ow eps x yuo Af Sapam nlp sew acd? hd meme eee 0 Sahn Mate My ogg Peete’ ee aa 
aoe, “Lahag wehbe, © ik Scenery again dnn | tetrapods tana etme mene 17 Soke a ph wa REPOS 6 


a mr 


| omncmannh 
myn tnetniriad iy te tries hth ath te ay teh Ak 4 Prt Rn at Ahoy 


) | AWE S Vig 
rons 


Ip, lagi 


Rha ny 
Se 


a ae 4 sie 
me 


Se tae ieee i ee Share tye beetudar a nt. we woke 





ee es 


ioe eg LN 
at , Ji eg hf 
rf y \ 7 52 ¥ t / \ ; q F 
he ce ie ; ‘oe 
Pk a a RTs oa ef Oh 


4 a 7 ri 
Oe Te Te Ve PR ee eee ere ee er 










PLEISTOCENE 


&DEVONIAN MIOCENE & RECENT 


a AN 


MISSISSIPPIAN 


=<" 





chiefly 
MI DDLE CAMBRIAN(?)- 


An 


LOWER CAMBRIAN() 





CAMBRIAN@) BELTIAN 


LEGEND 


Glacial drift and alhavium 


Kisheneln formation. 
chietly bluish-grey clay ; interbeds of 
grey sandstone; Ffossiliterous 





Limestone 
massive, grey, fossiliferous 


Roosville formation 
light green and gre}, thin-bedded metargihte 


| 


iNips formation. 
Pprrplish to red, thir-bedded metmyiliite & quatziti 








Gateway formation 
chiefly than-bedded, siliceous metargillite, 
some dolomite at base 





massive , basic flow 
Si 
Siyeh formation 
massive, dark grey, siliceous, magnesian 
Limestone, with much grecrishgrey meborgillite 
| 
| WwW 
[SLU CUBS SOSES | 
Wigwam formation. 
thin-to-thick-bedded red sandstone and metargillite 










Hefty formation 
chietly thick-bedded 


\ = 
Altyn formation 
thin-bedded siliceaus dolo 


Intrusive 





Abnormal] gabbro 


Symbols 


— 
| 


Geological boundary 





ae 








Glacial Striae 


Note. Locahties of chemically analyred 
rocks, shown thacs, +\|Z50 ‘ 















































sy Wigwam River 


Py 








Yy) 
Y SET 


a Pou es =o a 
a Sy BE NZ Sra SS? ze SY a AS ee 
5 = Ay . ( t \\ S Zee Lif; Y : ~ Mt 5) leg) 

ay 


_ 
































49° 








Topography from surveys made by 
the Boundary Commission. 













= =a 
a 









































Sea leve/ 





Section along line A B 


GEOLOGY OF THE FORTY-NINTH PARALLEL, ByR.A.Daly. 


Seale: 62500 —0:9864 Statute Miles tol Inch 
Miles 
1 Ye. oO . =~ 1 2 a 


MAP 75A 











Reprinted. by permission of Chief Astronomer, 


/ fe to accompany Geological Survey Memoir N° 36 
Contour trterval OO feet f ¢ 


se ipa ae pA eT it tl a a ne 


me A tS PE ee hE pe a eA mE 


An 
ereci< 


iy i Pale ne 
dé een th ee , 
Se 


nll af 
Werd, 


uke ten + id 
ee a ne ‘ 

3 y ae 

na ane ow 


ie a, : coms. F y ‘ 
2 eine Oe ea Pipe ee rere yee ee 
4 ; i — ne thes ety aa te 
a ean —s FS 


A ae 


’ 


Se os ~ a  e 
te ah cere en te 





& RECENT 


MIOCENE PLEISTOCENE 


chiefly 
MIDDLE CAMBRIAN@ 


—S oe ih) roe Eo 


BELTIAN LOWER CAMBRIAN(?) 
OSS 


CAMBRIAN( 


Sheet Nol 











LEGEND = ; — Se : SSS ew | 


- 








BRITISH COLUMBIA 

















i = : = = ——$———— 5 SS — —__—— ————— SSS 


STARVATION PEAK 
9300 









Glacial drift and alhawyviam 
inchuling winged-out moraines of the Flathead valley 









\isabanet ave 
Kishenehn formation. 
chiefly bliash-grey clays; interbeds 
of Grey sandstone;tossitferous 








———— 


chiefly tin-bedded jred_ argiltitejand 
interbedded flow of basic lava 


nes formation. 
chiefly, thin-bedded., b.ght gre. siticeous 
dolom t “a 


lorrute; amt wrterde w of basic lava 








He | 
Purcell lava 


massive, basic flow 











chiefly massive, dark grey, siliceous magnesia 
een also neuch greerash-grey metargiltite 





Gr 
Grimnell aS 
chietly thin-bedded ,red. metargilite; 
Titerbeddad low oP Baxia exiyg daloiw 

















ekunny formation 
TTA. tain-hedded , ght eerush.— y etargillite; 
pean etc Decree see 


ee 


Kut 













ta, Jake Ds 





Altyn formation 
Guarn-to thickbedded _ light grey, gy, sondy, siliceous, 
magnesia lwnestune; bearaw Fossil, “Beltivia dana 


Waterton i 


massive, dark grey, felspathized “dolomite 


GREAT DIVIDE 








P RIDGE 


























Intrusive 











\ 











Symbols 


are 


aa 
Geological boundary 


[PoreaeDi idelh en 








ishenehi Creek, 


| 


























Note. Localhities of chemically analyzed yd / 
rocks, shown thus, +\1306 ~ Sea Lleve —s —S = —— 










ee 
(01 Creek 


Great Plains MAP 74A 


n 











Reprinted by permisston of Chief Astronomer, 
to accompany Geological Survey Memowr N° 38 


“tical 











: eee ane ee AKBCDEF . 
GEOLOGY OF THE FORTY-NINTH PARALLEL, By R.A. Daly. 


Seale: 62500 — 0-9864 Statute Miles to | Inch 
Miles 














Contour interval, 100 feet 


ILLINOIS 


sam ATOM 


OF THE 


< 
UNIVERSITY OF 


PLateE 73. 





Columbia River terrace and the Pend D’Oreille mountains (Selkirk system). Looking southwest from near International Boundary. 





Typical view in the Midway Mountains. Looking northeastwardly across Kettle River near bridge six miles above Midway. 








Typical view in the Skagit range. Looking east from divide between Middle and Slesse creeks. Chilliwack River valley on the left. View shows accordance of summit levels. 


(In pocket.) 








UNIVERSITY OF ILLINOIS - 


ht : i 














(In pocket.) 


Typical view in the Clarke range. 


Looking eastward from head of Starvation Creek. The slope in middle of view is composed of the Siyeh formation capped by the Purcell Lava which is overlain by the Kintla formation. 


= 


Summit of the Nelson range (Selkirk system). 





Nelson range, looking west from summit ridge north of Dewdney trail. Ridges of near distance 





Looking north froma point a half-mile south of the Dewdney trail. Beehive Mountain distant, on the left. 








composed of vertical quartzites, etc., of the Summit serics. 


Prate 72. 


CLG “UOW JO 3SBO SOIIW GL"| SI EZ ” | 





” 
O22 ” ” S9c ” ” 
Lio ” ” v9 ” ” 
026 pees pinoys egg ” ” 
OLG “UD|A] JO ISOM SOjIWW HG"0 S! 69g ” ” 
89¢ ” ” 696 2” ” 
296 ”» ”» 19d ” ” 
992 ” ” 09¢ ” ” 
G96 a” 2? 69a ”? ” 
¥92 » 892 7) ” 
£96 ”? ” LGS ” ” 
G9 ” ” 996 ” ” 
L9% Gc ” ” =| y8GUS 
09¢ peal pjnoys acta ” ” 
8G0 “UO JO jSve Salil PL"g SI EGZ ” » 
89¢ Pees pjnoys Egg ” ” 
9G¢ “UOj JO 4SvO SOjl GG*? SI ZG% » ” | 
O90 Hasta | eGo ee : . 
GG ” ”» LG ” ” | 
¥SS 0S¢ ”? ” | 
eS¢ pees pinoys 606 ” ” H 
1G¢ “UO|A] JO [SBE Saj!ws Ge} SI Zaz » ” | 
Go» » 8b6 ”» » 
0ge » » L0G ” ” 
646» » Ob6 ” ” | 
8b ” ” Gra ” ” —G }98YS 
L9G ” ” bre 2” ” 
S¥e VS ” ” 
Sve peor pinoys Ove ” ” | 
Gye “UO JO SOM SOjIW Z?"O S! PHT ” ” 
€vo oy ”» Lye ” ” | 
Cve 5, ” Ove ” ” 
LVS 55 » 6&6 ” ” | 
Ove ” ” 8&3 ” ” | 
6&2» » L8S ”» ” | 
BES os » YES ” ” 
LEY ” ” Gm ” ” —"€E J@9US | 
98» » VES 5 9 
GES} ” ” S&S ” »” 
vES ”? ” CES ” ” 
£ES ” ” Lem ” ” 
GES ” ” O&¢ ” ” 
LES} ” ” 606 ” ” 
0&¢ ” ” 82d ”? ” 
660 £06 (penuizuod) 





8zz peel pinoys 92% jueunuo Ausepunoq —"p jooyus 





sdew—|j} wed 
OL6G} AQWOUOISY JeIUD 94} JO 
"9 xipusddy 
Vivuddad 


yodey 


L6G 
96¢ 
Goo 
GG 
E60 
6G 
Loe 
06d 


” 
2? 
” 
3? 
> 
9? 
3”? 


Loc 
026 
6LG 
1A 


6Le peo pinoys Zle 
Zig “UOW JO {See SOjILU ZO"O S! BIZ 


L136 
91e 
Glo 
VIS 
El’ 
(Ave 
LLo 
012 
606 


”? 
»” 
” 


” 


Ste 
Gla 
para 
Ele 
ole 
LL} 
OLS 
606 
802 


g0z pees pinoys 20g 
0% “UOIA] JO ISOM SEIU Z2°z 1 Z0Z 


v9l 
EOL 
cSt 
LOL 
O91 
6S 1 
8G 
2Gh 
OGL 
Sgt 
vGl 
esl 
eGh 
GL 
OSL 
6rl 
rl 
Lyl 
9FL 
Srl 


“191LUNC] AVOU 491} Aemjres OY} JO ySee SpseA MO} B SI GOL 


GOL 
POL 
e9t 
c9t 
LOL 
O9L 


OL 


br pecs pinoys Spt 
pejejep eq pjnous ppl 
Z0' | S169 

0g “Uo JO 3Somn Sol $6°G SI 6L juousnuow; Arepunog—"2| yeous 


09 "S93 


” 


bP 


3”? 


se Se 


—"b JOOUS 


—"g JOYS 


—"g 199US 


—"OL 
—'Gh 


” 
” 





, motte 
fl » es ae a 


v8 Ye) ODN Sigeyge 





‘yaoyS unjeLgq— 


‘S9SULY BPeISL>) PUL LIQUINIOZ) ‘YINYJIS ay} JO SMIIA—LL. , 
‘SOSUCY YIYTIS pue AYIOY 9} JO SMIIA—2L 9je[g 


‘aye] sewns—Zi se, 
OATS ORM el 
"95Uey WSeYS—SI 
‘g5uey UD9WIOZOF{—VI 
‘gsuey ueseueyOQ—tl 
‘uleyUNOY JaSsnIy[—ZI 
‘aye'yT sooOAOSO—II_,, 
‘suleyunopy ABMPIT—-O1 94S 


99 


9 


9) 


9) 


‘OyvT eursiiy7jy—O __e,, 

‘SUIEJUNOJA] PUL[SSOY— __e,, 

JIATY T9419, pusd—4 __,, 

‘Youaly [ja0ingG—9 

‘gsuey dAO[Y—S 

‘osuey yyeA—V se, 

‘youory, uleyUNOJ, AYIOY—* 
‘Q5uey UOWeD—Z eo, 

‘QHULY IYAIL[DJ—I 3V9yYS 


‘9 


PTE STOLL SZ, 


| 


URBANA 


IT 


119588835 


TTT 


il 


30112 


ate; 
ess 


Bib, Shad iongs Skea rae Bh 
we Re RALGR 
giitien oy SAS aaeoa 2 Fs 
A Rit amithneA Bore pore? Rp SRT Oe te 
= Sot 3 ae ‘ Seen 
peer 
peadepusn aaah 6) 


Sy SA RSL Ady J 35 . ‘5 ‘ es Sa ite arte as 


se a z i : Z pans taeeo" se? ieee ets : a ee, x + ‘ Sie: re 
pee asietisisies : “ ; CRRA Ress, : y oer 3 saree sRaes 


a 


Pneaialira te vtleg Aisle aie 
iaighy esate epee eegae 
ei ae sii a : ee ore ae 
Spriactsey ys ar ie eile 
ag iy tL 
é a ‘3 be By ase 
SaPEE FA TA 2 
Ni seo oe 


184, OA bee d 
Ami Irg ip wage 


Pyearevesty 2 ete te 





